- Dr. James GahertyDoherty Research ScientistLamont-Doherty Earth ObservatorySeismology Geology and Tectonophysics
1st Floor Seismology61 Route 9W - PO Box 1000PalisadesNY10964-8000USPhone:(845) 365-8450Fax:(845) 365-8150gaherty@ldeo.columbia.eduFields of interest:Earthquake Seismology, GeodynamicsThe surface of the Earth is constantly deforming, over time scales ranging from seconds to eons, and spatial scales ranging from centimeters to thousands of kilometers. This deformation fundamentally impacts human life by generating natural hazards such as earthquakes and volcanoes, as well as by modulating our natural environment and climate. The underlying cause of this deformation is convection in the Earths mantle, the large-scale circulation pattern where hot material is constantly cycled to the surface, where it cools and then sinks. In my research, I utilize seismic images of the Earths deep interior to gain a better understanding of mantle convection and its effect on Earths surface. This effort often requires collecting new seismic data in field locations ranging from the mountain peaks of far northwestern Canada, to the newly formed seafloor in the Gulf of California.
Honors & Awards:Sigma Xi Young Faculty Award, Georgia Institute of Technology 2002Lamont Projects:Selected Publications:The teleseismic signature of fossil subduction: Northwestern Canada, , Journal of Geophysical Research-Solid Earth, Apr 29, Volume 113, Issue B4, p.-, (2008), Doi 10.1029/2007jb005127
Seismic velocity structure and depth-dependence of anisotropy in the Red Sea and Arabian shield from surface wave analysis, , Journal of Geophysical Research-Solid Earth, Oct 14, Volume 113, Issue B10, p.-, (2008), Doi 10.1029/2007jb005335
Evaluating hot spot-ridge interaction in the Atlantic from regional-scale seismic observations, , Geochemistry Geophysics Geosystems, May 11, Volume 8, p.-, (2007), Doi 10.1029/2006gc001533
Surface wave tomography of the upper mantle beneath the Reykjanes Ridge with implications for ridge-hot spot interaction, , Journal of Geophysical Research-Solid Earth, Aug 24, Volume 112, Issue B8, p.-, (2007), Doi 10.1029/2006jb004785
Upper mantle structure beneath the eastern Pacific Ocean ridges, , Journal of Geophysical Research-Solid Earth, Jun 11, Volume 110, Issue B6, p.-, (2005), Doi 10.1029/2004jb003381
Mantle defomation during slow seafloor spreading constrained bv observations of seismic anisotropy in the western Atlantic, , Earth and Planetary Science Letters, Dec 15, Volume 228, Issue 3-4, p.255-265, (2004), DOI 10.1016/j.epsl.2004.10.026
Spreading-rate dependence of melt extraction at mid-ocean ridges from mantle seismic refraction data, , Nature, Dec 9, Volume 432, Issue 7018, p.744-747, (2004), Doi 10.1038/Nature03140
A surface wave analysis of seismic anisotropy beneath eastern North America, , Geophysical Journal International, Sep, Volume 158, Issue 3, p.1053-1066, (2004), DOI 10.1111/j.1365-246X.2004.02371.x
Structure of the Kaapvaal craton from surface waves, , Geophysical Research Letters, Jul 1, Volume 28, Issue 13, p.2489-2492, (2001)
Seismic evidence for hotspot-induced buoyant flow beneath the Reykjanes Ridge, , Science, Aug 31, Volume 293, Issue 5535, p.1645-1647, (2001)

